The Hall current system revealed as a statistical significant pattern during fast flows

We have examined the dawn-dusk component of the magnetic field, <I>B<sub>Y</sub></I>, in the night side current sheet during fast flows in the neutral sheet. 237 h of Cluster data from the plasma sheet between 2 August 2002 and 2 October 2002 have been analysed. The spat...

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Main Authors: K. Snekvik, R. Nakamura, N. Østgaard, S. Haaland, A. Retinò
Format: Article
Language:English
Published: Copernicus Publications 2008-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/3429/2008/angeo-26-3429-2008.pdf
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spelling doaj-2739b7fe4103438f8c88543bfe74e5182020-11-24T22:54:31ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-11-01263429343710.5194/angeo-26-3429-2008The Hall current system revealed as a statistical significant pattern during fast flowsK. Snekvik0R. Nakamura1N. Østgaard2S. Haaland3S. Haaland4A. Retinò5Department of Physics and Technology, University of Bergen, Bergen, NorwaySpace Research Institute, Austrian Academy of Sciences, Graz, AustriaDepartment of Physics and Technology, University of Bergen, Bergen, NorwayDepartment of Physics and Technology, University of Bergen, Bergen, NorwayMax-Planck-Institut für Extraterrestrische Physik, Garching, GermanySpace Research Institute, Austrian Academy of Sciences, Graz, AustriaWe have examined the dawn-dusk component of the magnetic field, <I>B<sub>Y</sub></I>, in the night side current sheet during fast flows in the neutral sheet. 237 h of Cluster data from the plasma sheet between 2 August 2002 and 2 October 2002 have been analysed. The spatial pattern of <I>B<sub>Y</sub></I> as a function of the distance from the centre of the current sheet has been estimated by using a Harris current sheet model. We have used the average slopes of these patterns to estimate earthward and tailward currents. For earthward fast flows there is a tailward current in the inner central plasma sheet and an earthward current in the outer central plasma sheet on average. For tailward fast flows the currents are oppositely directed. These observations are interpreted as signatures of Hall currents in the reconnection region or as field aligned currents which are connected with these currents. Although fast flows often are associated with a dawn-dusk current wedge, we believe that we have managed to filter out such currents from our statistical patterns.https://www.ann-geophys.net/26/3429/2008/angeo-26-3429-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. Snekvik
R. Nakamura
N. Østgaard
S. Haaland
S. Haaland
A. Retinò
spellingShingle K. Snekvik
R. Nakamura
N. Østgaard
S. Haaland
S. Haaland
A. Retinò
The Hall current system revealed as a statistical significant pattern during fast flows
Annales Geophysicae
author_facet K. Snekvik
R. Nakamura
N. Østgaard
S. Haaland
S. Haaland
A. Retinò
author_sort K. Snekvik
title The Hall current system revealed as a statistical significant pattern during fast flows
title_short The Hall current system revealed as a statistical significant pattern during fast flows
title_full The Hall current system revealed as a statistical significant pattern during fast flows
title_fullStr The Hall current system revealed as a statistical significant pattern during fast flows
title_full_unstemmed The Hall current system revealed as a statistical significant pattern during fast flows
title_sort hall current system revealed as a statistical significant pattern during fast flows
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-11-01
description We have examined the dawn-dusk component of the magnetic field, <I>B<sub>Y</sub></I>, in the night side current sheet during fast flows in the neutral sheet. 237 h of Cluster data from the plasma sheet between 2 August 2002 and 2 October 2002 have been analysed. The spatial pattern of <I>B<sub>Y</sub></I> as a function of the distance from the centre of the current sheet has been estimated by using a Harris current sheet model. We have used the average slopes of these patterns to estimate earthward and tailward currents. For earthward fast flows there is a tailward current in the inner central plasma sheet and an earthward current in the outer central plasma sheet on average. For tailward fast flows the currents are oppositely directed. These observations are interpreted as signatures of Hall currents in the reconnection region or as field aligned currents which are connected with these currents. Although fast flows often are associated with a dawn-dusk current wedge, we believe that we have managed to filter out such currents from our statistical patterns.
url https://www.ann-geophys.net/26/3429/2008/angeo-26-3429-2008.pdf
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